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(Mostly) Classical physics - PowerPoint Presentation

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(Mostly) Classical physics - PPT Presentation

of neutron star m agnetic fields Andreas Reisenegger Instituto de Astrofísica Pontificia Universidad Católica de Chile Workshop Astrosolids dense matter and gravitational waves Institute of Nuclear Theory U of Washington Seattle ID: 811062

stable amp magnetic time amp stable time magnetic toroidal hall neutron core fields field stratification equilibria diffusion braithwaite decay

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Slide1

(Mostly) Classical physics of neutron star magnetic fields

Andreas ReiseneggerInstituto de AstrofísicaPontificia Universidad Católica de Chile

Workshop

«

Astro-solids, dense matter, and gravitational waves»Institute of Nuclear Theory, U. of Washington, Seattle16-20 April 2018

Slide2

«ANSWERS»

group (as of 2016)Astrophysics

of Neutron Stars With Extra/Exotic/

Energetic/Extreme Related Stuffhttp://www2.astro.puc.cl/answers/

Funding:FONDECYT Regular

Grant

1150411

Rotational

& magnetic effects in neutron stars and beyond (2015-2019)FONDECYT postdoctoral grants, CONICYT PhD FellowshipsPFB-06 Center for Astronomy & Associated Technologies (CATA)

Slide3

Outline

Composition

gradients

& stable stratification Hydromagnetic equilibria & stabilityProcesses in the neutron star crust: Hall + OhmCore B evolution: eroding stable stratificationApplication: weak B of LMXBs & MSPs

Conclusions

&

discussion

Slide4

Magnetic field in neutron stars??

In vacuum (lab), neutrons decay with half-life ~ 15 min:In dense, degenerate matter, low-energy quantum states are filled (blocked) “Chemical” (weak interaction) equilibrium:

Around nuclear density, neutrons coexist with some protons & electrons: Density-dependent fraction, few %Charged & degenerate: currents flow with very little resistance

 Magnetic field “frozen in” for a long time (Baym et al. 1969)

Slide5

Composition gradient in NS

core

Possible

e

quilibrium particle populations in very dense matter Glendenning,Compact Stars, p. 239

Slide6

Stratification & buoyancy

Non-barotropic fluid:

blob displaced from equilibrium “remembers” where it came from,

through its composition (in NSs) or specific entropy (main sequence, WDs)

Brunt-Väisälä

(buoyancy)

frequency> 0: stable oscillations (“g-modes”)< 0: unstable

convection

= 0: neutrally stable (“barotropic”)

“Ledoux criterion”

Slide7

Stable stratification vs. B

Slide8

Hydromagnetic equilibria 

Slide9

Axially symmetric equilibriaPoloidal+toroidal decomposition:

2 scalars  (r, ) & 

(r, ) Each component independently satisfies

No fluid forces in  - direction: Thus,

2 types of toroidal “magnetic surfaces” of constant  &  :closing outside the star:  = 0: pure poloidal field

closed

inside

the star:   0: twisted toroidal field

Braithwaite 2007

Slide10

Stability??

Purely toroidal (azimuthal) fields are unstable

Flux rings “repel” each other (Tayler 1973)

Figure

from Spruit 1999

Slide11

Purely poloidal (meridional) fields

are also unstable

Braithwaite 2008

Slide12

Stable MHD equilibria

MHD

simulations

:

(Braithwaite & Spruit 2004, 2006; Braithwaite 2009)Self-gravitating balls of conducting fluidStably stratified by an entropy gradientDisordered initial BGeneric outcome ~ axially symmetric: Poloidal & toroidal B

components

stabilize

each other

Slide13

Effect of stable stratification

Mitchell, Braithwaite, Reisenegger, Spruit, Valdivia, & Langer 2015 Random initial B Ordered initial B

(twisted torus)

Warning:

Ratio of diffusive/Alfvén time strongly reduced in the simulations!

In

stably stratified

stellar models, we find configurations that decay slowly (~diffusion time

 MHD-stable) & others that decay quickly (~Alfvén time  unstable). In barotropic models, all configurations explored decay quickly.

Diffusion

only

Stable

Strat.

Barotropic

Stable

Strat.

Slide14

Stability condition &

hidden energy

(

Very

rough) conditions for mutual stabilization of Bpol vs. Btor :

Braithwaite

2009; Marchant+ 2011; Akgün+ 2013; Mitchell+ 2015

Possibly strong, hidden toroidal BEnergy reservoir for magnetars (Thompson & Duncan 2001), especially «low‐B magnetars» (Rea+ ‘10, ‘12, ‘13)Non‐uniform surface temperature on CCOs (Shabaltas & Lai 2012)Continuous gravitational waves (Cutler 2002; Mastrano+ 2011; many more)

 

Will

these

equilibria

live

forever

?

Slide15

Solid NS crust: Hall + Ohm

 

Slide16

NS crust: Hall drift

Hall drift non-linear  “turbulent

cascade” to small scales

? (Goldreich & R. 92)Analytic solutions:Current

sheets (Vainshtein et al. 2000; Reisenegger et al. 2007)Large-scale Hall equilibria (Gourgouliatos et al. 2013)Numerical 2D (= axial symmetry): Stable Hall equilibria = “attractors” (Gourgouliatos & Cumming 14a,b; Marchant et al. 14; Cumming et al. in prep.); braking indices n<3 (Gourgouliatos & Cumming 14c)

Coupled

thermo-magnetic

evolution: Viganò et al. 13Numerical 3D: Attractors appear to survive (Wood & Hollerbach 15)All this assumes that the magnetic flux goes only through the crust

Unlikely

unless

a

core

superconductor can

expel

the

flux (time

scale

???)

Either

way

,

need

to

study

processes

in

the

core

Slide17

(Multi-)

fluid core

B pushes on the fluid (charged particles): Can it escape??Not trivial: Stable stratification (composition gradient) prevents (or strongly constrains) bulk motions.Ways out:

Bulk motion with “real-time” composition adjustment through beta decays (mUrca): n  p + e Effective at high T (& B): magnetars (Thompson & Duncan 1996)

Ambipolar diffusion (solenoidal mode): Relative motion of 2 fluids: neutrons & charged particles (frozen to B) against their mutual collisions Effective at low T: old NSs ~ progenitors of LMXBs & MSPs? [Time scales: Goldreich & R. 1992; 1D sim.: Hoyos, R., & Valdivia 2008, 2010]

Slide18

Simulation (Castillo+ 2017): axial

symmetry (meridional cut) charged particles & B moving

against a fixed, uniform neutron backgroundMagnetic

field Density/pressure Velocity field

Slide19

Simulation results & discussionB evolves towards twisted-torus equilibria

 No full decayBUT: Still to be included

:Radial density gradientsNeutron motionAdditional particle

speciesSuperconductivity (type I or II??) & superfluidity3D effects: likely instabilities!

Slide20

Low B in MSPs & LMXBs

Standard explanation:

«Recycling» via

accretion reduces not only

P, but also B, through either:1) Accretion

heating

enhanced crustal resistivity (Shibazaki+ 1989): requires B not to penetrate the core2) Diamagnetic

screening

by

accreted

material (

Bisnovatyi-Kogan

&

Komberg

’74; Melatos++;

many

others

):

instabilities

??

(

Mukherjee

+ 2013)

Alternative

(

toy

model

-- Cruces, R., & Tauris, in

prep

.):

Spontaneous

decay

by

ambipolar

diffusion

of

core

field

in

cold

pre-

accretion

phase

(

requires

crust

to

«

cooperate

»)

Time

available

~

companion’s

main

sequence

lifetime

infer

from

remnant

Slide21

Magneto-roto-thermal evolution

Massive

, short-

lived companion(now neutron

star)Low-mass, long-lived companion(now He white dwarf)Cruces, R., & Tauris, in preparation

Slide22

Magnetic fields of binary pulsars

Histogram: Binary pulsars

not in globular clusters

Shaded bands:

Rough estimates of expected fields for ambipolar diffusion for each companion

type

,

with

(companion’s main sequence lifetime) – (NS cooling time) (106 yr) = (ambipolar diffusion time)

Caveats

:

Several

outliers

:

unusual

binary

evolution

?

P

redictions

similar

to

«

standard

»

accretion-induced

decay

model

Slide23

Conclusions & discussion

B

fields

are «weak» (ε ~ 10-6 B152)Their stability depends on:Linked poloidal & toroidal componentsStable stratification of core matter  Allows for a strong, hidden toroidal component

Secular

evolution

through non‐ideal MHD processes:Ohmic resistivity in the crustNon-linear Hall dynamics in the crustErosion of stable stratification in core  destabilization of equilibria  Explanation of weak MSP/LMXB fields?Still no full simulations or understanding:3D instabilities?Ubiquity & effects of superfluidity or superconductivity?